SEA [si:]

SEA的基本解释

n.

海, 海洋

-

=special effect amplifier 特殊效果放大器

相似词

sea

与SEA相关的情景对话

商务外贸 / 发货

A:

How do you like the goods dispatched, by railway or by sea?

你方将怎样发运货物，铁路还是 海运 ？

B:

By sea, please. Because of the high cost of railway transportation, we prefer sea transportation.

请 海运 发货，铁路运输费用太高，我们愿意走 海运 。

A:

That's what we think.

我们正是这么想的。

商务外贸 / International Trade-Shipping-(国际贸易-运输)

A:

Hello, I’m calling from San Francisco for Kevin Lee.

哈啰，我从旧金山打来找李凯文。

B:

This is Kevin Lee speaking.

我是李凯文。

A:

Hi. This is Helen Parker calling.

嗨。我是海伦.派克。

B:

Good morning, Helen. What can I do for you?

早安， 海伦。有什么我能效劳的吗？

A:

I'm calling to find out how you would like your order of speakers, by air or by sea?

我想请教你要如何运送你下单的扬声器，空运还是海运?

B:

We need part of that order by next week, so we would like to do a partial air shipment.

我们下个星期就要一部分的订货，所以我们有部份想用空运。

A:

How much of it do you want shipped by air?

您想要空运多少数量呢?

B:

We'd like to ship half the order by air and the rest by sea.

一半用空运，剩下的一半用海运。

A:

OK. Do you want us to use our freight forwarding agent?

好的。你要用我们公司的货运代理商吗?

B:

Actually, we've got a freight forwarder over there-China Consolidated. I'll fax you their contact information.

事实上，我们这边自己有货运公司--中国联合公司。我会把他们的联络资料传真给你。

A:

All right. We can deliver that half to your agent tomorrow morning.

好的。我们明早可以出一半的货给你们的代理商。

B:

That would be great.

那样很好。

A:

I'm not sure what the shipping schedule will be for the sea freight.

我不确定海运的时间表。

B:

No hurry. We're not in a big rush for the second half of the order.

不急。另一半的订单我们不是很急。

A:

All right. I'll let you know the shipping details later and I'll send you the shipping documents by DHL as soon as I get them.

好的。我稍后再通知你送货细节，我一拿到出货文件就马上用DHL 快递给你。

B:

Very good. We'll be expecting to hear from you. And thanks for calling.

很好。我们等你的消息。谢谢你的来电。

与SEA相关的网络例句 [注：此内容来源于网络，仅供参考]

According to the energy conservation theory, BOM and CSIM4 were coupled. The BOM has no treatment on transmission solar radiation, which is of great importance when the model is adapted to Arctic Ocean. So the treatment was introduced to BOM. Through numerical test on different lead albedos, it was found that sea ice thickness is not so sensitive to lead albedo, which may be contribute to the lead occupies little ratio within multiyear sea ice pack. The reason of summer over-melt of arctic sea ice is the NCEP reanalysis downward solar radiation being larger than its reality. Then the arctic sea ice climate variability was simulated. Results showed that: simulated ice thickness change is in accord with the submarine investigated mean sea-ice draft changes. Simulated annually maximum ice thickness along the Eurasian continental oceans are closely related to the observed ones. The long-term mean simulated ice motion has the same features of the SSM/I derived ice motion. Sea ice extents in differential sub-regions have same trends comparing to the satellite passive-microwave data derived ones. Simulated ice concentration is closely related to the observed in the Arctic sub-regions. Sea ice flux through the Fram Strait involves ice concentration, motion and thickness. It is a composite criterion for sea ice model evaluation. The simulated ice area and volume export through the strait accord with the satellite derived or statistically reconstructed ones.(5) The simulated ice thickness climate variability and mean sea surface current of the coupled model were analyzed, results showed: the total ice volume in the Arctic Ocean has a significant decreasing trend. The volume variability is of a 10-year timescale oscillation, with two major periods of 12-13a and 18-20a. Mean ice thickness in the arctic sub-seas has different tendencies. It has an increasing trend in the Barents-Kara Sea and Baffin Bay-Labrador Sea, and decreasing in the others. The characteristic time scale of 7-10a wherein the river discharges leads the Fram Strait ice volume export is about the period that river water takes to be conveyed across the Arctic Ocean.(6) Using the simulated ice distribution in the Arctic Ocean and China precipitation, air temperature and SST in tropical key regions, the climate teleconnection were studied. Result showed: When the mean sea ice thickness is large in the central Arctic Ocean and Chukchi-Beaufort Sea , and small in the Barents-Kara Sea and Baffin Bay-Labrador Sea , the precipitation in South China, Tibetan Plateau, and the north part of Northeastern China are always smaller than normal, and v. v. When the mean ice thickness is small in CA, BC, East Siberian Sea and Greenland-Iceland-Norwegian Sea , and large in BL, The air temperature in north-eastern China, the southern of Tibetan Plateau, and Hainan Island, are always lower than normal, and v. v. In addition, when the sea ice is thick in BC and BL, the SST is larger in the middle and eastern Pacific Ocean, and is smaller in the tropical Southeastern Indian Ocean.

由于BOM没有考虑透射太阳辐射的物理过程，研究表明透射太阳辐射对北冰洋的能量收支起到重要作用，因此在BOM模式中引入了对透射太阳辐射的处理；通过对不同水道反照率的数值试验表明海冰厚度对水道反照率的敏感性不强，可能与海冰区水道面积占的比率很小有关；而模式模拟的北极海冰夏季&过度融化&主要源于NCEP再分析资料提供了偏大的太阳短波辐射；对北极海冰的气候变率进行了模拟研究，结果表明：模拟的海冰厚度变化与潜艇探测的海冰吃深度变化具有一致性；模拟和观测的亚欧大陆沿海的年内最大海冰厚度有很好的相关；模拟的海冰移速与长期平均的卫星反演的海冰移速具有相同的速度分布特征；模拟的各个海区海冰面积的变化趋势与卫星反演资料分析的结果基本一致；模拟与观测的主要海洋分区的海冰密集度具有很好的相关：弗瑞姆海峡的海冰体积和面积的输送涉及到海冰密集度、厚度和移动速度，是判断模式模拟能力的一个综合的指标，模式模拟的结果与卫星反演或重建的面积输送、体积输送具有很好的一致性；(5)分析了模拟的北极海冰厚度的气候变率及气候平均表层海流场，结果表明：北极海冰的总体积有显著减少的趋势，北极海冰总体积的变化具有10a际尺度振荡的特点，存在18-20a和12-13a两个主周期；北极海冰的平均厚度在各个海区的变化趋势不同，在巴伦支—喀拉海和巴芬湾—拉布拉多海地区海冰厚度有显著的增加趋势，而其它海区存在减少的趋势；通过对模拟的气候平均表层海流的分析表明，北极河流流量超前弗瑞姆海峡海冰流量7-10年的特征时间尺度与表层海流的气候分布存在着必然联系：(6)利用模拟结果以及中国降水、气温和热带关键区SST资料，讨论了北极各海区海冰平均厚度与中国降水、气温以及热带关键区SST的关系，结果表明：在北极中心海区和楚科奇—波弗特海海冰厚度偏大，在巴伦支—喀拉海以及巴芬湾—拉布拉多海海冰厚度偏小，则中国降水在华南地区、青藏高原和东北北部降水偏少，反之相反；在北极中心海区、东西伯利亚海、楚科奇—波弗特海以及格陵兰海海冰厚度偏小，在巴芬湾—拉布拉多海海冰厚度偏大，则在中国东北地区、高原南部地区和海南岛附近气温偏低，反之相反；另外，北极楚科奇—波弗特海和巴芬湾—拉布拉多海海冰厚度偏大时，在热带中东太平洋海温偏高，而在热带东南印度洋海温偏低。

Sea ice severe degree and disaster in Bohai Sea from 1950 through 2007 promulgated by State Oceanic Administration People's Republic of China has been summarized. According to these reports and bulletins involved with sea ice severe degree and disaster, the statistical means of 5-year moving average are applied, the feedback of sea ice disaster to the societal activity in every National Five-year Plan has been exhibited, the relation between sea ice disaster and sea ice severe degree has been quantificationally analyzed. Some conclusions have been derived as follows: sea ice disaster appeared proportionably to industrial activity and sea ice severe degree, but inverse proportionnably to the understandings of cognition of defending in sea ice disasters; so that the weaken sea ice conditions could not inevitably result in the loosening of sea ice disaster.

通过归纳整理1950年以来渤海海冰冰情等级以及国家海洋局公报内的海冰灾害，并应用五年滑移平均，以反映中国"五年计划"的社会活动与海冰灾害之间的响应，定量分析海冰灾害发生率同海冰冰情等级的关系，发现工业活动的频繁程度同海冰灾害发生率成正比；人类重视程度同海冰灾害发生率成反比；海冰冰情等级与海冰灾害发生率成正比；当海冰冰情等级减轻时，海冰灾害发生率并不一定减少。

The northern side is the white ream sea, a gram of the 鄂霍 sea, Japanese sea, Yellow sea, the east the china sea and south china sea; go toward the south is the huge east India islands to be divided into the ocean Su pulls the 威 west sea, the Java sea and Timor sea;Became the coralline sea and tower 斯曼 sea again in Australia.

北面是白令海，鄂霍次克海，日本海，黄海，东中国海和南中国海；往南是巨大的东印度群岛把大洋分成了苏拉威西海，爪哇海和帝汶海；在澳洲又形成了珊瑚海和塔斯曼海。

与SEA相关的网络解释 [注：此内容来源于网络，仅供参考]

sea：海

则具有作出必要的修改后的相应含义;"输入"、"进口"(import) 指输入香港;"进口商"(importer) 指有关油类在输入时的报关人(不论是他本人或由别人代表他报关);"油"、"油类"(oil) 指原油及燃油;(10)在本条中,"海"(sea) 不包括<<释义及

sea：海洋

第五节 - 货物和其它物品的抵达、逗留和离开54 在5.3推荐做法中,以postal items两词代替"mail"一词(中文均为邮件,故不修改),并在"海洋"(sea)和"应该"(should)两词之间增加"或进口"(or importation).

sea：大海

朗格斯酒庄坐落于素有"中国酿酒葡萄之乡"美称的河北昌黎,与地处渤海湾风景如画的碣石山和黄金海岸为邻,全面融合了兴建葡萄酒庄的3S原则: 大海(SEA) 沙滩(SAND) 阳光(SUN) 朗格斯酒庄(秦皇岛)有限公司以创建人朗格斯先生的名字命名,

sea：西雅图

UDI) 西雅图 (SEA) 悉尼 (SYD) 夏洛特 (CLT) 辛辛那提 (CVG) 新加坡 (SIN) 休斯顿 (IAH) 雅典 (ATH) 雅加达 (CGK) 亚的斯亚贝巴 (ADD) 亚特兰大 (ATL) 盐湖城 (SLC) 伊丽莎白港 (PLZ) 伊斯兰堡 (ISB) 伊斯坦布尔 (IST) 印第安纳波利斯 (IND) 约翰内斯堡 (JNB) 札幌 (CTS) 芝加哥 (ORD) 中国香港特别行政区 (HKG) 出发 返回

sea：abbr. strategy environmental effect appraisal; 战略环境影响评价